rocks were it not for the unceasing thunder, far below,
from the bottom of the Rajah Fall. The next rapid
to be crossed is that of the Roarer, which takes, before
it goes over the precipice a most singular course—first
flowing into a basin at the edge of the cliff, and
then leaving this in a northerly direction, after
which it rushes down a steep stony trough to fall into
the same deep pool which receives the water of the
Rajah Fall. After crossing the bridge of the
Roarer rapid the bed of the river has again to be traversed
and at a distance of about 700 feet you reach the
rapid of the Rocket. This is a fall of wonderful
beauty, for the water projects itself sheer from the
cliff to fall about 100 feet on to a vast projecting
piece, or rather buttress of rock, which causes the
water to shoot out into a rocket-like course from
which are thrown off wonderfully beautiful jets, and
arrowy shoots of water, and spray, and foam, which
seem to resemble falling stars or shooting meteors.
You then pass over another section of the river bed
for about 500 feet till you reach the rapid, or rather
stream, of the la Dame Blanche Fall which glides gently
over the precipice in a broad foaming silvery sheet.
From the first rapid to the last the distance is about
733 yards. I have met with no estimate of the
total width of the fall when the river is in full
flood, but it can hardly be less than half a mile
wide, and the depth of the water, as one can see from
the high water mark, must be very great. It is
interesting to note on the tops of the boulders here
and there the circular stones that have, during each
monsoon, been whirling round and round, each one in
its own pothole.
After crossing the last bridge you then walk over
the rocks into the forest beyond and strike the path
which leads down through the forest on the Mysore
side of the river, to a point called Watkin’s
platform—an open-sided shed about 100 feet
below the top of the falls, and which commands a view
of the gorge below the falls, and a fair, though rather
distant view of the falls. When approaching the
platform I was positively startled by a vast shrieking
clang which suddenly burst on the ear and seemed to
fill the air. This I afterwards found had come
from the semi-cavernous gorge of rock about half a
mile away, into which fall the waters of the Rajah
and Roarer rapids, and though I afterwards heard somewhat
similar sounds issuing from these falls, I never heard
again anything approaching to this singular and startling
burst of sound. These sounds have often been
remarked upon, but no one seems to have attempted
to trace their cause, but they most probably arise
from the escape of air which has been driven by the
falling waters into some deep fissures of the rock.